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Science lesson plan · 9th grade (Year 10 in England) · 60 minutes

How Earth's atmosphere changed over time

Earth and rocks

CCSS NGSS.HS-ESS2-7CCSS NGSS.HS-ESS1-6England: GCSE Combined Science: Chemistry of the atmosphere

Objective and success criteria

Students will: How Earth's atmosphere changed over time.

  • I can answer questions on today's skill on my own, without help.
  • I can explain each step and say why it works.
  • I can check my answer and spot a mistake.

Before and after

Needs first: The Earth's atmosphere; Earth's 4.6-billion-year history on a timeline

Leads to: the next skill in this area.

Materials: Rock samples, Hand lenses, Mini whiteboards, A diagram or short video clip of the idea, Printed student sheet (below).

Warm-up · 6 min

  • Quick retrieval from earlier learning (The Earth's atmosphere; Earth's 4.6-billion-year history on a timeline). Students answer on mini whiteboards.
  • Show answers together and note who needs support in the main task.
  1. Which gas makes up most of the air we breathe? (hydrogen / carbon dioxide / oxygen / nitrogen) → nitrogenPrompt: It is about four-fifths of the air.
  2. What happened to much of the carbon dioxide in the early atmosphere? (It dissolved in oceans and was locked up in rocks and fossil fuels / It is all still in the air / It escaped to the Moon / It turned into nitrogen) → It dissolved in oceans and was locked up in rocks and fossil fuelsPrompt: Think of limestone, coal and oil.
  3. Where did most of the oxygen in today's atmosphere come from? (volcanoes / the oceans boiling / photosynthesis by algae and plants over billions of years / the Sun) → photosynthesis by algae and plants over billions of yearsPrompt: Early Earth had almost no oxygen.

Hook · 6 min

  • Pass round different rocks and ask how each one might have formed.
  • Share the objective: How Earth's atmosphere changed over time. Read the success criteria together.

I do: model it · 12 min

  • Work through the example out loud, saying why you do each step, not just what you do.
  • Example: Today's dry air is about 78 % nitrogen and 21 % oxygen. What percentage is made up of all the other gases together?
  • Step 1: 100 − 78 − 21 = 1
  • Step 2: So the answer is: 1 %
  • Answer: 1 %
  • Pause after each step and ask a student to say what comes next.

We do: guided practice · 12 min

  • Do these together. Students try each step on whiteboards before you reveal it.
  • Use the hints as prompts rather than giving the answer.
  1. Today's dry air is about 78 % nitrogen and 21 % oxygen. What percentage is made up of all the other gases together? → 1 %Prompt: Percentages of all the gases add up to 100.
  2. Why did the amount of carbon dioxide in the early atmosphere decrease? (Volcanoes absorbed it / It escaped into space / It dissolved in oceans, was used in photosynthesis and was locked in rocks and fossil fuels / It turned into nitrogen) → It dissolved in oceans, was used in photosynthesis and was locked in rocks and fossil fuelsPrompt: More than one process removed it.

You do: independent practice · 17 min

  • Students work on the student sheet. Circulate and check the first two answers of every student early.
  • Students who finish: write a question of their own for a partner, with the answer.

The 8 questions are on the student sheet below, with answers in the key.

Exit ticket · 7 min

  • Two questions on their own. Sort answers into got it / nearly / not yet to plan the next lesson.
  1. Dry air is about 21 % oxygen. In 400 cm³ of air, roughly what volume is oxygen, in cm³? → 84 cm³Prompt: To find a percentage of an amount, multiply and divide by 100.
  2. Scientists think the early atmosphere was mostly carbon dioxide, like Venus and Mars today. Why are they not certain? (Nobody has studied rocks / The atmosphere has never changed / Venus has no atmosphere / There is limited direct evidence from billions of years ago) → There is limited direct evidence from billions of years agoPrompt: Think about how old the evidence would have to be.

Watch out for

  • Everyday meanings of words getting in the way of the science meaning: define key words explicitly.
  • Remembering facts without the reason: ask "why?" and "what is the evidence?"

Support and stretch

Support

  • Review first: The Earth's atmosphere.
  • Use concrete materials: rock samples.
  • Give the first step of each question, or a partly worked example to finish.
  • Pair with a confident partner for the guided practice.

Stretch

  • Explain a common mistake in writing and how to fix it.
  • Write a word problem that uses today's skill, then solve a partner's.

Homework and more practice

Free online practice with hints and printable worksheets for this skill: eurekami.com/science/grade-9.

Free lesson plan from eurekami.com/lesson-plan-builder

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How Earth's atmosphere changed over time

Name

Date

Score/ 8

  1. Question 1

    Dry air is about 21 % oxygen. In 500 cm³ of air, roughly what volume is oxygen, in cm³?

    Answercm³

  2. Question 2

    Why did the amount of carbon dioxide in the early atmosphere decrease?

    • A. It escaped into space
    • B. Volcanoes absorbed it
    • C. It dissolved in oceans, was used in photosynthesis and was locked in rocks and fossil fuels
    • D. It turned into nitrogen
  3. Question 3

    Dry air is about 21 % oxygen. In 200 cm³ of air, roughly what volume is oxygen, in cm³?

    Answercm³

  4. Question 4

    Today's dry air is about 78 % nitrogen and 21 % oxygen. What percentage is made up of all the other gases together?

    Answer%

  5. Question 5

    Where did most of the oxygen in today's atmosphere come from?

    • A. melting ice
    • B. volcanic eruptions
    • C. photosynthesis by algae and plants over billions of years
    • D. meteorites
  6. Question 6

    Dry air is about 78 % nitrogen. In 400 cm³ of air, roughly what volume is nitrogen, in cm³?

    Answercm³

  7. Question 7

    Which gas makes up most of today's atmosphere?

    • A. argon
    • B. carbon dioxide
    • C. nitrogen
    • D. oxygen
  8. Question 8

    Dry air is about 21 % oxygen. In 400 cm³ of air, roughly what volume is oxygen, in cm³?

    Answercm³

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Answer key: How Earth's atmosphere changed over time

  1. 1. 105 cm³

  2. 2. C. It dissolved in oceans, was used in photosynthesis and was locked in rocks and fossil fuels

  3. 3. 42 cm³

  4. 4. 1 %

  5. 5. C. photosynthesis by algae and plants over billions of years

  6. 6. 312 cm³

  7. 7. C. nitrogen

  8. 8. 84 cm³